Abstract
Flash
floods
are
largely
driven
by
high
rainfall
rates
in
convective
storms
that
projected
to
increase
frequency
and
intensity
a
warmer
climate
the
future.
However,
quantifying
changes
future
flood
flashiness
is
challenging
due
lack
of
high-resolution
simulations.
Here
we
use
outputs
from
continental
convective-permitting
numerical
weather
model
at
4-km
hourly
resolution
force
hydrologic
scale
depict
such
change.
As
results
indicate,
US
becoming
7.9%
flashier
end
century
assuming
high-emissions
scenario.
The
Southwest
(+10.5%)
has
greatest
among
historical
flash
hot
spots,
central
(+8.6%)
emerging
as
new
spot.
Additionally,
flood-prone
frontiers
advancing
northwards.
This
study
calls
on
implementing
climate-resilient
mitigation
measures
for
spots.
Water Resources Research,
Journal Year:
2020,
Volume and Issue:
57(3)
Published: Nov. 14, 2020
Abstract
This
paper
is
derived
from
a
keynote
talk
given
at
the
Google's
2020
Flood
Forecasting
Meets
Machine
Learning
Workshop.
Recent
experiments
applying
deep
learning
to
rainfall‐runoff
simulation
indicate
that
there
significantly
more
information
in
large‐scale
hydrological
data
sets
than
hydrologists
have
been
able
translate
into
theory
or
models.
While
growing
interest
machine
sciences
community,
many
ways,
our
community
still
holds
deeply
subjective
and
nonevidence‐based
preferences
for
models
based
on
certain
type
of
“process
understanding”
has
historically
not
translated
accurate
theory,
models,
predictions.
commentary
call
action
hydrology
focus
developing
quantitative
understanding
where
when
process
valuable
modeling
discipline
increasingly
dominated
by
learning.
We
offer
some
potential
perspectives
preliminary
examples
about
how
this
might
be
accomplished.
Global Change Biology,
Journal Year:
2017,
Volume and Issue:
23(8), P. 2941 - 2961
Published: March 20, 2017
Abstract
Climate,
physical
landscapes,
and
biota
interact
to
generate
heterogeneous
hydrologic
conditions
in
space
over
time,
which
are
reflected
spatial
patterns
of
species
distributions.
As
these
distributions
respond
rapid
climate
change,
microrefugia
may
support
local
persistence
the
face
deteriorating
climatic
suitability.
Recent
focus
on
temperature
as
a
determinant
insufficiently
accounts
for
importance
processes
changing
water
availability
with
climate.
Where
scarcity
is
major
limitation
now
or
under
future
climates,
likely
prove
essential
persistence,
particularly
sessile
plants.
Zones
high
relative
–
mesic
microenvironments
generated
by
wide
array
processes,
be
loosely
coupled
therefore
buffered
from
change.
Here,
we
review
mechanisms
that
their
robustness
We
argue
will
act
species‐specific
refugia
only
if
nature
space/time
variability
compatible
ecological
requirements
target
species.
illustrate
this
argument
case
studies
drawn
California
oak
woodland
ecosystems.
posit
identification
could
form
cornerstone
climate‐cognizant
conservation
strategies,
but
would
require
improved
understanding
change
effects
key
including
frequently
cryptic
such
groundwater
flow.
Abstract
Predictions
of
floods,
droughts,
and
fast
drought‐flood
transitions
are
required
at
different
time
scales
to
develop
management
strategies
targeted
minimizing
negative
societal
economic
impacts.
Forecasts
daily
seasonal
scale
vital
for
early
warning,
estimation
event
frequency
hydraulic
design,
long‐term
projections
developing
adaptation
future
conditions.
All
three
types
predictions—forecasts,
estimates,
projections—typically
treat
droughts
floods
independently,
even
though
both
extremes
can
be
studied
using
related
approaches
have
similar
challenges.
In
this
review,
we
(a)
identify
challenges
common
drought
flood
prediction
their
joint
assessment
(b)
discuss
tractable
tackle
these
We
group
into
four
interrelated
categories:
data,
process
understanding,
modeling
prediction,
human–water
interactions.
Data‐related
include
data
availability
definition.
Process‐related
the
multivariate
spatial
characteristics
extremes,
non‐stationarities,
changes
in
extremes.
Modeling
arise
analysis,
stochastic,
hydrological,
earth
system,
modeling.
Challenges
with
respect
interactions
lie
establishing
links
impacts,
representing
interactions,
science
communication.
potential
ways
tackling
including
exploiting
new
sources,
studying
a
framework,
influences
compounding
drivers,
continuous
stochastic
models
or
non‐stationary
models,
obtaining
stakeholder
feedback.
Tackling
one
several
will
improve
predictions
help
minimize
impacts
extreme
events.
This
article
is
categorized
under:
Science
Water
>
Hydrological Sciences Journal,
Journal Year:
2018,
Volume and Issue:
63(5), P. 696 - 720
Published: March 22, 2018
Two
approaches
can
be
distinguished
in
studies
of
climate
change
impacts
on
water
resources
when
accounting
for
issues
related
to
impact
model
performance:
(1)
using
a
multi-model
ensemble
disregarding
performance,
and
(2)
models
after
their
evaluation
considering
performance.
We
discuss
the
implications
both
terms
credibility
simulated
hydrological
indicators
adaptation.
For
that,
we
confirm
hypothesis
that
good
performance
historical
period
increases
confidence
projected
under
change,
decreases
uncertainty
projections
models.
Based
this,
find
second
approach
more
trustworthy
recommend
it
assessment,
especially
if
results
are
intended
support
adaptation
strategies.
Guidelines
global-
basin-scale
period,
as
well
criteria
rejection
from
an
outlier,
also
suggested.
Hydrology and earth system sciences,
Journal Year:
2021,
Volume and Issue:
25(7), P. 3897 - 3935
Published: July 7, 2021
Abstract.
Hydroclimatic
extremes
such
as
intense
rainfall,
floods,
droughts,
heatwaves,
and
wind
or
storms
have
devastating
effects
each
year.
One
of
the
key
challenges
for
society
is
understanding
how
these
are
evolving
likely
to
unfold
beyond
their
historical
distributions
under
influence
multiple
drivers
changes
in
climate,
land
cover,
other
human
factors.
Methods
analysing
hydroclimatic
advanced
considerably
recent
decades.
Here
we
provide
a
review
drivers,
metrics,
methods
detection,
attribution,
management,
projection
nonstationary
extremes.
We
discuss
issues
uncertainty
associated
with
approaches
(e.g.
arising
from
insufficient
record
length,
spurious
nonstationarities,
incomplete
representation
sources
modelling
frameworks),
examine
empirical
simulation-based
frameworks
analysis
extremes,
identify
gaps
future
research.
EarthArXiv (California Digital Library),
Journal Year:
2020,
Volume and Issue:
unknown
Published: Feb. 11, 2020
We
suggest
that
there
is
a
potential
danger
to
the
hydrological
sciences
community
in
not
recognizing
how
transformative
machine
learning
will
be
for
future
of
modeling.
Given
recent
success
applied
modeling
problems,
it
unclear
what
role
theory
might
future.
central
challenge
hydrology
right
now
should
clearly
delineate
where
and
when
adds
value
prediction
systems.
Lessons
learned
from
history
motivate
several
clear
next
steps
toward
integrating
into
workflows.
Journal of Applied Meteorology and Climatology,
Journal Year:
2019,
Volume and Issue:
58(4), P. 663 - 693
Published: Jan. 30, 2019
Abstract
The
Canadian
Regional
Climate
Model
(CRCM5)
Large
Ensemble
(CRCM5-LE)
consists
of
a
dynamically
downscaled
version
the
CanESM2
50-member
initial-conditions
ensemble
(CanESM2-LE).
downscaling
was
performed
at
12-km
resolution
over
two
domains,
Europe
(EU)
and
northeastern
North
America
(NNA),
simulations
extend
from
1950
to
2099,
following
RCP8.5
scenario.
In
terms
validation,
warm
biases
are
found
EU
NNA
domains
during
summer,
whereas
winter
cold
appear
NNA,
respectively.
For
precipitation,
generally
wetter
than
observations
but
slight
dry
also
occur
in
summer.
change
projections
for
2080–99
(relative
2000–19)
show
temperature
changes
reaching
8°C
summer
some
parts
Europe,
exceeding
12°C
northern
Québec
winter.
central
will
become
much
dryer
(−2
mm
day
−1
)
(>1.2
).
Similar
observed
although
drying
is
not
as
prominent.
Projected
interannual
variability
were
investigated,
showing
increasing
decreasing
winter,
Temperature
increase
by
more
70%
80%
northernmost
part
month
May
snow
cover
becomes
subject
high
year-to-year
future.
Finally,
CanESM2-LE
CRCM5-LE
compared
with
respect
extreme
evidence
that
higher
allows
realistic
representation
local
extremes,
especially
coastal
mountainous
regions.
Earth System Dynamics,
Journal Year:
2019,
Volume and Issue:
10(1), P. 91 - 105
Published: Feb. 13, 2019
Abstract.
The
rationale
for
using
multi-model
ensembles
in
climate
change
projections
and
impacts
research
is
often
based
on
the
expectation
that
different
models
constitute
independent
estimates;
therefore,
a
range
of
allows
better
characterisation
uncertainties
representation
system
than
single
model.
However,
it
known
groups
share
literature,
ideas
representations
processes,
parameterisations,
evaluation
data
sets
even
sections
model
code.
Thus,
nominally
might
have
similar
biases
because
similarities
way
they
represent
subset
or
be
near-duplicates
others,
weakening
assumption
estimates.
If
there
are
near-replicates
some
models,
then
treating
all
equally
likely
to
bias
inferences
made
these
ensembles.
challenge
establish
degree
which
this
true
any
given
application.
While
issue
recognised
by
many
community,
quantifying
accounting
dependence
anything
other
an
ad-hoc
challenging.
Here
we
present
synthesis
disparate
attempts
define,
quantify
address
common
conceptual
framework,
provide
guidance
how
users
can
test
efficacy
approaches
move
beyond
weighted
ensemble.
In
upcoming
Coupled
Model
Intercomparison
Project
phase
6
(CMIP6),
several
new
closely
related
existing
anticipated,
as
well
large
from
models.
We
argue
quantitatively
addition
performance,
thoroughly
testing
effectiveness
approach
used
will
key
sound
interpretation
CMIP
future
scientific
studies.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(6), P. 1673 - 1693
Published: March 31, 2022
Abstract.
Deep
learning
is
becoming
an
increasingly
important
way
to
produce
accurate
hydrological
predictions
across
a
wide
range
of
spatial
and
temporal
scales.
Uncertainty
estimations
are
critical
for
actionable
prediction,
while
standardized
community
benchmarks
part
model
development
research,
similar
tools
benchmarking
uncertainty
estimation
lacking.
This
contribution
demonstrates
that
can
be
obtained
with
deep
learning.
We
establish
procedure
present
four
baselines.
Three
baselines
based
on
mixture
density
networks,
one
Monte
Carlo
dropout.
The
results
indicate
these
approaches
constitute
strong
baselines,
especially
the
former
ones.
Additionally,
we
provide
post
hoc
analysis
put
forward
some
qualitative
understanding
resulting
models.
extends
notion
performance
shows
learns
nuanced
behaviors
account
different
situations.